Fig. 4From: Elastostatic effects around a magma reservoir and pathway due to historic earthquakes: a case study of Mt. Fuji, Japan a–e Map view of volumetric strain changes due to earthquakes. The dotted lines represent isograms of volumetric strain changes in each of the five earthquake scenarios (Fig. 3) at a depth of 20 km beneath Mt. Fuji. The unit is 1 μ strain. Positive values indicate dilation, and negative values indicate compression. The orange solid triangle, orange open triangle, red broken line, and blue squares have the same meanings as in Fig. 2 Back to article page